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<br />n ." "f'f"'S' <br />'J .) ;,/ ,.J ,J <br /> <br />25 <br /> <br />90" <br /> <br />85" <br /> <br />CHRONOLOGY OF THE 1976-77 DROUGHT <br /> <br />75' <br /> <br /> <br />48' <br /> <br />t <br /> <br />WISCONSIN <br /> <br />44' <br /> <br />o <br />I <br />o <br /> <br />80. <br /> <br />EXPLANATION <br /> <br />- Region boundary <br /> <br />44. <br /> <br />PENNSYLVANIA <br /> <br />40' <br /> <br />'"0 <br />I <br /> <br />200 KI LOMETERS <br />I <br />I <br />100 MILES <br /> <br />Figure 9. Great Lakes-WRC Region 04. <br /> <br />but rainfall for June through October 1977 <br />ranged from 75 to 150 percent of normal. <br />The Palmer index (see figs. 6 and 7) re- <br />flects the precipitation distribution in time <br />and space mentioned above and the fact that <br />above normal precipitation did not always end <br />drought conditions because agriculture is de- <br />pendent upon rain at roughly weekly intervals <br />as well as an adequate amount of rain. No <br />significant rain fell in Wisconsin between <br />Apri115 and May 11, 1977. The Palmer index <br />for the Upper Peninsula of Michigan dropped <br />to -4 or lower in August 1976 and stayed near <br />that for more than a year. Values this low <br />indicate extreme drought conditions. Northern <br />Wisconsin and northeastern Minnesota had Pal- <br />mer indexes ranging from -4 to -9 at one time <br />or another between August 1976 and August <br />1977. <br />Above normal temperatures during the <br />summer of 1976 intensified the drought con- <br />ditions primarily by reducing the soil moisture. <br />Then the very low temperatures during the <br />severe winter of 1976-77 made it necessary to <br /> <br />run water through pipes to keep them from <br />freezing and further taxed the dwindling water <br />supply and the pumping capacity of a few <br />cities. Unseasonably high temperatures and <br />strong winds the latter part of April 1977 in <br />Wisconsin reduced the soil moisture to 25 per- <br />cent of normal. <br />The low precipitation in 1976, the very cold <br />winter of 1976-77, and the continuation of <br />below normal precipitation in 1977 were a <br />series of events in which each succeeding <br />event compounded the effects of the earlier <br />events. Together they made the drought the <br />most serious one in at least 50 years in Michi- <br />gan, Minnesota, and Wisconsin. <br />The runoff pattern in Wisconsin reflected <br />the precipitation pattern very closely. By <br />early August 1976, the flows in the northwest <br />basins had dropped to amounts that past <br />records show have been exceeded 92 percent <br />of the time. Flows in the Fox-Wolf River <br />basin south and west of Green Bay were <br />approaching the 10-yr low flow by late August <br />1976. <br />